Qp Structure of Sediments in the Kanto Plain
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概要
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The QP structure was derived for the sediments and the uppermost crust in the Kanto plain. Synthetic explosion seismograms were computed for causally attenuative crustal models with the elastic wave velocities determined by refraction experiments, and they were compared with observed seismograms. After some forward and inverse modelings we obtained an optimal QP structure, in which sedimentary layers have very low Qp-values of 35 and 100, as against 400 for the uppermost crust.
- 東京大学地震研究所,Earthquake Research Institute, University of Tokyo,地震研究所の論文
- 1986-03-31
東京大学地震研究所,Earthquake Research Institute, University of Tokyo,地震研究所 | 論文
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